The contribution of aerosols to light extinction at Meadview, AZ, during su
mmer 1992 was estimated using Mie theory and size-resolved aerosol chemical
measurements. Sulfate particle size increased as a function of relative hu
midity. Twelve-hour average light scattering was estimated to within 15%. S
ulfate was the most abundant chemical component in the fine aerosol fractio
n. On average, Rayleigh scattering, coarse particles, and fine sulfates con
tributed 39, 21, and 19% to total light extinction. Average estimated light
scattering was largely insensitive to assumptions about mixing state, degr
ee of sulfate neutralization and organic carbon water uptake properties. It
was estimated that a reduction of Mohave Power Plant (MPP) SO2 emissions c
orresponding to a contribution of 19% to ambient sulfate would have resulte
d in a decrease in total light extinction of between 3.3 and 5.3%. (C) 2000
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